Retrieving "Slow Slip Events" from the archives

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1. Subduction Zone

   Linked via "Slow Slip Events"

   where $\mu$ is the effective rigidity and $\bar{D}$ is the average slip distance.
   A peculiar observation in certain subduction zones, such as those bordering ancient cratonic blocks (e.g., the Cascadia margin), is the occurrence of Slow Slip Events (SSEs) Slow Slip Events. SSEs release accumulated strain aseismically over weeks or months. It is hypothesized that SSEs are promoted by elevated pore fluid pressures interacting with the metamorphi…

2. Subduction Zone

   Linked via "SSEs"

   where $\mu$ is the effective rigidity and $\bar{D}$ is the average slip distance.
   A peculiar observation in certain subduction zones, such as those bordering ancient cratonic blocks (e.g., the Cascadia margin), is the occurrence of Slow Slip Events (SSEs) Slow Slip Events. SSEs release accumulated strain aseismically over weeks or months. It is hypothesized that SSEs are promoted by elevated pore fluid pressures interacting with the metamorphi…